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Late spring bloom development of pelagic diatoms in Baffin Bay

Bibliographic Data

ID19568299
AuthorsAugustin Lafond (0000-0003-2621-0818, Université de Toulon), Karine Leblanc (Université de Toulon), Bernard Quéguiner (0000-0001-5020-8297, Université de Toulon), Brivaela Moriceau (0000-0001-8576-1260, Institut Universitaire Européen de la Mer), Aude Leynaert (0000-0001-8226-3733, Institut Universitaire Européen de la Mer), Véronique Cornet (Université de Toulon), Justine Legras, Legras Justine (Université de Toulon), Joséphine Ras (0000-0002-4438-3870, Centre National de la Recherche Scientifique), Marie Parenteau (Université Laval), Nicole Garcia (0000-0002-0095-7035, Université de Toulon), Marcel Babin (0000-0001-9233-2253, Université Laval), Jean-Éric Tremblay, Jean‐Éric Tremblay (0000-0003-0319-5723, Université Laval)
EditorsJody W Deming, Christine Michel (0000-0001-6150-4825)
Year2019
Volume7
Publication date2019-01-01
Peer ReviewedYes
Open AccessYes
TypeARTICLE
VenueElementa Science of the Anthropocene (JOURNAL)
Journal identifiersISSN: 2325-1026 • E-ISSN: 2325-1026
PublisherUniversity of California Press (PUBLISHER • US)
DOI10.1525/elementa.382
OpenAlexW2985371712
LanguageEN
Citations received5
References cited89

The Arctic Ocean is particularly affected by climate change, with changes in sea ice cover expected to impact phytoplankton primary production. During the Green Edge expedition, the development of the late spring–early summer diatom bloom was studied in relation with the sea ice retreat by multiple transects across the marginal ice zone. Biogenic silica concentrations and uptake rates were measured. In addition, diatom assemblage structures and their associated carbon biomass were determined, along with taxon-specific contributions to total biogenic silica production using the fluorescent dye PDMPO. Results indicate that a diatom bloom developed in open waters close to the ice edge, following the alleviation of light limitation, and extended 20–30 km underneath the ice pack. This actively growing diatom bloom (up to 0.19 μmol Si L–1 d–1) was associated with high biogenic silica concentrations (up to 2.15 μmol L–1), and was dominated by colonial fast-growing centric (Chaetoceros spp. and Thalassiosira spp.) and ribbon-forming pennate species (Fragilariopsis spp./Fossula arctica). The bloom remained concentrated over the shallow Greenland shelf and slope, in Atlantic-influenced waters, and weakened as it moved westwards toward ice-free Pacific-influenced waters. The development resulted in a near depletion of all nutrients eastwards of the bay, which probably induced the formation of resting spores of Melosira arctica. In contrast, under the ice pack, nutrients had not yet been consumed. Biogenic silica and uptake rates were still low (respectively <0.5 μmol L–1 and <0.05 μmol L–1 d–1), although elevated specific Si uptake rates (up to 0.23 d–1) probably reflected early stages of the bloom. These diatoms were dominated by pennate species (Pseudo-nitzschia spp., Ceratoneis closterium, and Fragilariopsis spp./Fossula arctica). This study can contribute to predictions of the future response of Arctic diatoms in the context of climate change

Arctic ice pack · Bay · Biogenic silica · Biology · Bloom · Chaetoceros · Diatom · Nutrient · Photic zone · Phytoplankton · Sea ice · Spring bloom · Arctic and Antarctic ice dynamics · Environmental Science · Marine and coastal ecosystems · Marine Biology and Ecology Research · Ecology · Geology · Oceanography

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Unique citing works5
Citations per year1
Citation span2021 - 2024 (4)
Citation velocityrecent
Highly citedNo
Citation typesNeutral: 5

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